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Geological Formation

Vinschgau

Valleys

Vinschgau, also called Val Venosta in Italian, is the upper part of the Adige (Etsch) river valley in the western part of South Tyrol, Italy, running from the Merano basin east to the Reschen Pass in the northwest. The valley is bordered by the Ötztal Alps to the north and other Alpine ranges to the west and south. The district, established in 1962, comprises 13 municipalities centered on Schlanders, covers about 1,442 square kilometers, and has a population of roughly 35,000. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

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Caused By

Erosion, Processes

Wikidata P31 formation-type mapped to formative process Erosion via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Vinschgau

In Discipline

Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Vinschgau
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Also in Geography Atlas: where this subject is found.

Source Wikidata: Vinschgau
Sources
Vinschgau (Wikipedia)
Lead section
Quote, Lead section
The Vinschgau, Vintschgau (German: [ˈfɪn(t)ʃɡaʊ]) or Vinschgau Valley (Italian: Val Venosta [ˈval veˈnɔsta]; Romansh: Vnuost [ˈfnuɔ̯ʃt] ; Ladin: Val Venuesta; medieval toponym: Finsgowe) is the upper part of the Adige or Etsch river valley, in the western part of the province of South Tyrol, Italy.
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Wikidata: Vinschgau
Wikidata Q1468834, class allow-list match (w-wdresolver-0926)View the Source
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